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Difference between revisions of "Olivine"

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'''Olivine''' is one of many low [[value]] minerals that are [[magma-safe]], and can be used for floodgates and mechanisms used for the controlling of magma. It is also one of the few minerals that contains [[native platinum]] (the other being [[magnetite]]).
 
'''Olivine''' is one of many low [[value]] minerals that are [[magma-safe]], and can be used for floodgates and mechanisms used for the controlling of magma. It is also one of the few minerals that contains [[native platinum]] (the other being [[magnetite]]).
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Items built using olivine will be dark green.
 
Items built using olivine will be dark green.
  
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==In the real world==
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==In real life==
 
Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)<sub>2</sub>SiO<sub>4</sub>.
 
Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)<sub>2</sub>SiO<sub>4</sub>.
 
It is defined by its bright green color. Gem-quality examples of the mineral are called [[peridot]].
 
It is defined by its bright green color. Gem-quality examples of the mineral are called [[peridot]].

Revision as of 01:40, 15 July 2014

!!UNKNOWN!!  · xTATTEREDx  · +FINE+  · *SUPERIOR*  · ≡EXCEPTIONAL≡  · ☼MASTERWORK☼
Olivine
OlivineSample.png
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Uses

Location

  • Found within gabbro as large clusters
Properties
Fire-safe Magma-safe

Wikipedia article

v50.14 · v0.47.05
This article is about the current version of DF.
Note that some content may still need to be updated.

Olivine is one of many low value minerals that are magma-safe, and can be used for floodgates and mechanisms used for the controlling of magma. It is also one of the few minerals that contains native platinum (the other being magnetite).

Items built using olivine will be dark green.

In real life

Olivine is a magnesium iron silicate mineral with the chemical formula (Mg,Fe)2SiO4. It is defined by its bright green color. Gem-quality examples of the mineral are called peridot.

It is also the most common rock in the world, taking up an estimated 80% of the world's volume, of course most of this is in the mantle 7km underground in the sea and an average 35km beneath the continent. Even dwarves can't dig that far down.

  • Green sand, or fragmented olivine. Some fragments are loose and some are visibly still embedded in the black lava rock below

  • A small olivine piece

  • Brighter olivine

  • Olivijn.gif

    Small olivine pieces

  • Olivine, clear high quality crystals are called peridot if they are gem-quality

  • Another sample of olivine/peridot

V · T · E
Sedimentary
Igneous
Intrusive
Extrusive
Metamorphic
Ore
Economic
Other
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